Monger W H (22 results)
Anatomy of North America: Thematic Geologic Portrayals of the Continent (FROM: Tectonophysics, Vol. 187, 1991, PP. 117-134 + folded plate.
Williams, Harold, Paul F. Hoffman, John F. Lewry, James W. H. Monger and Toby Rivers.
Published by Elsevier Publishing Company., 1991
- Softcover
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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Add to basketNo Binding. Condition: Good. ORIGINAL Reprint/Offprint of journal article; includes folded plate w/ 6 tectonic maps of North America; inscribed by Harold Williams; light creasing of corners of leaves; o/w in good condition. Journal.
Published by Geology, 1982
- Softcover
- Magazine / Periodical
Seller: Larry W Price Books, Portland, OR, U.S.A.Larry W Price Books
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Add to basketPamphlet. Condition: Very Good. Vol 10, No 2, pp. 70-75, Illus, 4to, Extracted from orig vol, thus begins with title page, trimmed & stapled pamphlet, else VG.
Published by Geological Survey of Canada Paper 67-42, 1968, 39 Pp. + Folded Map in Rear Pocket., 1968
- Softcover
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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Add to basketSoft Cover. Condition: Very Good. Softcovers; ex-corporate library; minor shelfwear w/ light creasing of corners of wraps and leaves; o/w in very good condition.
Published by Geological Survey of Canada Paper 68-48, 1969, 41 Pp. + Loosely-Inserted Map., 1969
- Softcover
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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Add to basketSoft Cover. Condition: Good. Softcovers; ex-corporate library; minor shelfwear w/ small creases at corners of wraps and a few leaves; small tear on lower edge of rear wrap; light glue stain on last leaf due to facing library card; o/w in good condition.
Language: English
Published by Geological Survey of Canada, Ottawa, ON, Canada, 1968
- Softcover
Seller: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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US$ 7.32
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Add to basketSoft cover. Condition: Very Good +. Geological Survey of Canada Paper 67-42. 39pp. Folded map in rear pocket collated to Contents. Titled card wrapper is clean and without wear. Stapled binding sound. Reduced shipping may apply.
Language: English
Published by Geological Survey of Canada, Ottawa, ON, Canada, 1973
- Softcover
Seller: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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US$ 10.98
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Add to basketSoft cover. Condition: Very Good +. Geological Survey of Canada Paper 70-33. v, 71pp. Folded map and figure in rear pocket collated to Contents. Titled card wrapper is clean and without wear. Stapled binding sound. Reduced shipping may apply.
Contributions to Canadian Paleontology (Five Papers)
B.S. Norford and Reuben J. Ross, Jr.; T.T. Uyeno; Charles A. Ross and E.W. Bamber; Charles A. Ross and J.W.H. Monger; Charles A. Ross
Language: English
Published by Geological Survey of Canada, Ottawa, ON, Canada, 1978
- Softcover
Seller: Post Horizon Booksellers, Nokomis, SK, CanadaPost Horizon Booksellers
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Add to basketSoft cover. Condition: Very Good. Geological Survey Bulletin 267. 75pp. Green card wrapper clean and without wear. Stapled binding sound. Papers: New species of brachiopods and trilobites from the Middle Ordovician (Whiterock) of southeastern British Columbia (Norford, Ross); Some Late Middle Devonian (Polygnathus varcus Zone) c…onodonts from central Mackenzie Valley, District of Mackenzie (Uyeno); Middle Carboniferous and Early Permian fusulinaceans from the Monkman Pass area, northeastern British Columbia ( Ross, Bamber); Carboniferous and Permian fusulinaceans from the Ominica Mountains, British Columbia (Ross, Monger); Permian fusulinaceans from the St. Elias Mountains, Yukon Territory (Ross).
Published by USGS, Denver, CO, 1999
- Softcover
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Add to basketCondition: very good. from the introduction, "We interpret a Phanerozoic tectonic model of the Circum-North Pacific for the orogenic collages along the eastern margin of the North Asian Craton and the western margin of the North American Craton." softcover, 11" x 8.5", 122 pages, illustrated.
Language: English
Published by Washington D.C.: American Geophysical Union, 1987
- Hardcover
Seller: Antiquariat Thomas Haker GmbH & Co. KG, Berlin, GermanyAntiquariat Thomas Haker GmbH & Co. KG
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Hardcover/Pappeinband. Condition: Gut. 165 pages. Good. Ex-library with usual markings. Clean pages. Cover shows mild wear. Sprache: Englisch Gewicht in Gramm: 890.
Published by The Geological Soceity of America, 1985
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Add to basketCondition: very good. from the introduction, "This pamphlet supplements the display sheets of Transect B2. It provides (1) descriptions of terranes on the line of Transect B2, (2) comments on gravity, magnetic and heat flow data and seismicity by R. P. Riddihough, (3) description of the seismic cross-section by R. M. Clowes, (4)… bases for the compilation of Cross-section II and (5) references." DT3. pictorial envelope, dup written in marker on cover, text 20 pages stapled, Two large folded maps, scale 1:500,000.
Language: English
Published by American Geophysical Union/Geological Society of America, 1987
- Hardcover
Seller: Anybook.com, Lincoln, United KingdomAnybook.com
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Condition: Good. Volume 18. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Clean from markings. In good all round condition. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,850grams, ISBN:087…5905196.
Published by Department of Energy, Mines and Resources, 1973
- Softcover
Seller: The Bookseller, Edmonton, AB, CanadaThe Bookseller
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Add to basketStapled Wraps. Condition: Very Good-. Minor shelf wear. Owner name and date on front cover. Otherwise a square, tight, unmarked book. v, 71 pp. 2 folded maps in rear pocket.
Published by USGS, 2005
- Softcover
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Condition: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV2. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
- Softcover
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Condition: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Condition: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea." DV4. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
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Condition: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western Nor…th American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. DX1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Published by USGS, 2005
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Condition: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western Nor…th American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Language: English
Published by Ottawa, Department of Energy, Mines and Resources, 1975
- Softcover
Seller: Antiquariat Bookfarm, Löbnitz, GermanyAntiquariat Bookfarm
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Add to basketSoftcover. Condition: Gut. w30877 'MPX' Geological Survey of Canada. Nr. 74-47. Upper Paleozoic Rocks of the Atlin Terrane, Northwestern British Columbia and South-Central Yukon. (5 Karte + 1 Erl.) Sprache: Englisch Gewicht in Gramm: 450.
Published by Department of Energy, Mines and Resources, Ottawa, Canada, 1975
- Softcover
Seller: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Add to basketPaperback. Condition: Very Good. Unmarked, except for enclosing envelope, which contains stamps and some scribbling. Envelope is torn and slightly damaged on one edge and some corners show wear. Book and maps are well preserved. ; Book Description; Spine has no signs of creasing. Pages are clean and not marred by notes or folds.… Covers are square with minor wear. Ships Safe and Fast. ; Paper - Geological Survey of Canada ; 74-47; B&W Illustrations; 4to 11" - 13" tall; 63 pages DE4.
Language: English
Published by Geological Association of Canada, Vancouver, British Columbia, Canada, 2003
- Softcover
Seller: Bay Used Books, Sudbury, ON, CanadaBay Used Books
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Soft cover. Condition: Good. Moderate wear. Binding fairly tight, pages clean. Pictures available upon request.
Mesozoic Stratigraphy and Jurassic Paleontology West of Harrison Lake, Southwestern British Columbia - Bulletin 441
Arthur, Andrew John; Geological Survey of Canada; Smith, Paul L.; Monger, W.H.; Tipper, Howard W.
- Softcover
- First Edition
Seller: RareNonFiction, IOBA, Ladysmith, BC, CanadaRareNonFiction, IOBA
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Paperback. Condition: Very Good. First Edition. 62 pages. "This detailed study of the lithostratigraphy and biostratigraphy of the strata permits a reconstruction of much of the history of sedimentation, volcanism, plutonism, uplift and erosion during Mesozoic time in the Coast Mountains, an area commonly devoid of stratigraphic… sections with reliable fossil control. In this bulletin several fossil groups are used to date the various lithological units that can be traced into the plutonic complex." - from Preface. Two figures stored in pocket. Light wear. Minimal library markings. A quality copy.
Published by Government of Canada, Ottawa, 1994
- Softcover
- First Edition
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Add to basketPaperback. Condition: Fair. First Edition. 316 pages. Bibliography. Black and white plates, maps and line drawings. Heavily worn with usual library markings. Binding intact. Title page removed.
